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Well-exposed soft-sediment deformation (SSD) structures occur in Tecopa paleolake beds largely composed of ash from the Bishop (760kyr) and the Lava Creek (640kyr) ultra-plinian eruptions. In both cases the SSD structures affected volcaniclastic deposits concentrated by overland flow from the surrounding topography into the lower slope and lake environments. Re-sedimentation of ash produced alternations...
Early Pleistocene lacustrine deposits of the Baza Basin in SE Spain show a 2 m thick sheet with deformation structures intercalated within horizontal strata. Along a 180 m exposure we recognise an alternation of compressional (thrusts) and extensional (normal faults and tensional joints) structures. These structures are interpreted as a planar slump. Analysis of the different structures together with...
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